Additional seminars that Petrel RobertsonConsulting Ltd. will run on request:

Fluvial Deposits of the Brazeau-Belly River Sequence,Alberta Foothills and Subsurface,

West-Central Alberta

CHANNEL RESERVOIRS AND ASSOCIATEDDEPOSITS OF WESTERN CANADA

(Core Seminar)Channel reservoirs are difficult to find and understand, butoffer assets with high economic impact. In addition to formingprolific reservoirs, channel fills and related deposits also areimportant in aiding petroleum entrapment within flanking non-channelized units. Furthermore, the complex architecture ofsome channelized deposits creates torturous fluid flow pathswithin reservoirs, which greatly influences reservoirdevelopment schemes like waterflooding, EOR, horizontal welltrajectories, and perforation programs.

The complexstratigraphy andsedimentology

mandates asophisticatedknowledge of therocks forming bothreservoir and non-reservoir strata.This seminar exposes participants to a large spectrum ofproductive, prospective and trapping strata. Participants willreview deposits of braided, meandering estuarine, andanastomosed systems. They will observe channel fill, pointbar and crevasse-splay reservoirs, trapping units in tightchannel fill sandstone and mudstones, and reservoirheterogeneities associated with non-reservoir interbeds andintraformational breccia.

ofchannel filldeposits locatedwithin thesubsurface ofwestern Canada

MESOZOIC RESERVOIR SANDSTONESOF WEST-CENTRAL ALBERTA (Core Seminar)

Prospect development andefficient reservoir exploitationrely upon detailed knowledgeof reservoirs, seals, and theirrelationships in thesubsurface. The study ofcores remains the mostfundamental and powerfultool in developing thisknowledge, and provides thebasis for application of othersubsurface imagingtechnologies.

The complex stratigraphy and sedimentology of the numerousprospective Mesozoic reservoir sandstones in west-centralAlberta makes a comprehensive knowledge of the rocksessential. This seminar exposes participants to a wide spectrumof productive, prospective, and trapping strata located betweenTownships 30 and 70, west of the fifth meridian. We will reviewreservoir units deposited in fluvial and estuarine channel, tidalflat, shoreface, and shelfal environments. Trapping strata includecemented sandstones, as well as impermeable overbank,interfluve, and marine deposits.

Participants are exposed to the spectrum ofproductive and trapping units foundassociated with Lower Cretaceous clasticheavy oil and tar sand reservoirs in Alberta(these deposits are directly analogous tobeds located in west-central Saskatchewan).

Following a lecture on the geology of theheavy oil-tar sand belt, participants will spendmost of two days viewing cores from thegeneral Lloydminster-Cold Lake-Wabasca-Peace River-Athabasca regions. The coresselected will cover the complete stratigraphicspectrum of Lower Cretaceous (Mannville)units as well as the varying types of reservoirarchitecture, including channel fills, estuarinedeposits, and wave-formed shorelines.

CLASTIC HEAVY OIL AND TAR SANDRESERVOIRS (Core Seminar)

GEOMETRY AND KINEMATICS OF SELECTEDHYDROCARBON-TRAPPING, NON-

CONTRACTIONAL STRUCTURAL REGIMES

This two day lecture series will focus on the geometry andkinematics of tectonic regimes that have been the focus of newhydrocarbon play concepts..

Coupled Shelf Extensional and basin directed“toe-thrust” Systems

Strike/Oblique-SlipFault Zones.

Day 1:. There have been several significant

hydrocarbon discoveries in deep water toe-thrust systems,associated with the mobilization of salt and/or shale. The firstday of this lecture series will examine in detail both salt- andshale-based toe-thrust systems. Established examples that willbe reviewed include WestAfrica (Niger Delta, Angola),Gulf of Mexico (Gulf ofCampeche), East CoastIndia (Krishna Gadavari),and Brunei (Bram Delta).The MacKenzie Delta andEast Coast Africa, tworegimes that may yet beclassified as toe-thrustsystems, will also bediscussed.

Day 2:Exploration

along strike/oblique-slip faultsystems has traditionallyfocused on mappingstructural traps related toen-echelon folding and contractional oblique-slip faults (e.g.southern California). More recently, the association ofhydrothermal dolomites with deep-seated strike-slip fault zones(e.g. northern Alberta, northeast BC, Anticosti Basin, Albion-Scipio of Michigan, Ellenberger-Texas) has generated newplays. The key issues are the relationships between strike-slipfault zones, heat-flow anomalies, fluid flow and fracturenetworks. This second day lecture will examine the kinematicsof strike-slip fault zones based on their map patterns ofstructures of various sizes.

MODERN AND ANCIENT CLASTICSHORELINE DEPOSITS, WILLAPA BAY AREA,

WASHINGTONMany productive units in Western Canada are interpreted tobe the products of marine shoreline deposition. In thisdepositional setting, great lateral and vertical complexity isto be expected within and between reservoirs.Understanding their complexities is crucial to effectiveexploration and reservoir development. In order tounderstand these deposits one needs to appreciate thedepositional dynamics and the distribution of the severalsub-environments associated with shoreline deposits.Ideally, one should be exposed to both outcrops andmodern depositional systems. In outcrop, one sees thevertical and lateralvariability, whereasobservation ofmodern sedimentsgives insight intoactive processes andsedimentdistributions at thesurface.

Petrel Robertson'sfield seminar to theWillapa Bay area ofWashington isunique in that participants not only view modern sedimentsbut also analogous Late Pleistocene deposits which areexposed in cliffs found at the shoreline.

Besides the benefits to geologists, this field seminar shouldalso be of interest to both geophysicists and reservoirengineers. Geophysicists will be able to see the relativescale, lateral continuity and complexity of wave-formed andtidal sediments. Engineers will observe the depositionalprocesses associated with marine shorelines and therebyget an appreciation of the number, type and extent of non-random heterogeneities found in shoreline reservoirs.

Petrel Robertson Consulting Ltd.FIELD AND CORE

SEMINARSVisit www.petrelrob.com

for details of our field and core seminarsor phone Leslie Sears at +1-403-218-1618

Seminars are not scheduled regularly, butwe will run any of these seminars at clientrequest. Focused sessions can bedesigned to meet the particular interestsof a client group.

TIGHT GAS SANDSTONE RESERVOIRS OF THEWESTERN CANADIAN SEDIMENTARY SHIELD

(A Core Seminar)Until recently, Canadian tight gas production has been dominatedby the hunt for stratigraphic “sweet spots”, where pockets ofconventional reservoir quality can be produced within a tight gasfairway, and which drain some of the encasing tight gas sandstonefacies. During the past few years, however, advances in drillingand completions and economies of scale have allowed gasproducers to access gas stored in low-permeability, truly “tight”sandstone reservoirs.

Petrel Robertson’s Tight Gas Sandstone core review addressesboth stratigraphic sweet spot reservoirs (and their encasing tightfacies), and tight (sub-millidarcy) clastic reservoirs. Specific coresessions can be assembled to address the specific needs ofclients. Examples are drawn from PRCL’s non-exclusive study“Comparative Evaluation of Tight Gas Play Opportunities, WCSB”,which addresses 13 stratigraphic intervals and 24 play types.These include: Tight, organic-rich siltstones (Montney and DoigFrms); locally fractured calcareous sandstones (Rock Creekmember); stratigraphic and fractured sweet spots along extensiveconglomerate/sandstone fairway (Cadomin Frm); stratigraphicsweet spots in coarser, cleaner valley-fill sandstone facies(Glauconitic member and Spirit River Frm); stratigraphic sweetspots on conglomeratic shoreline trends (Falher and NotikewinMbrs, Cadotte Frm); stratigraphic sweet spots associated withearly chlorite clay rims and locally fractured tight shorefacesandstones (Cardium Frm).

One- or two-day tight gas core sessions can be customized forany client group.